the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
How accurate are estimates of glacier ice thickness? Results from ITMIX, the Ice Thickness Models Intercomparison eXperiment
Daniel Farinotti
Douglas J. Brinkerhoff
Garry K. C. Clarke
Johannes J. Fürst
Holger Frey
Prateek Gantayat
Fabien Gillet-Chaulet
Claire Girard
Matthias Huss
Paul W. Leclercq
Andreas Linsbauer
Horst Machguth
Carlos Martin
Fabien Maussion
Mathieu Morlighem
Cyrille Mosbeux
Ankur Pandit
Andrea Portmann
Antoine Rabatel
RAAJ Ramsankaran
Thomas J. Reerink
Olivier Sanchez
Peter A. Stentoft
Sangita Singh Kumari
Ward J. J. van Pelt
Brian Anderson
Toby Benham
Daniel Binder
Julian A. Dowdeswell
Andrea Fischer
Kay Helfricht
Stanislav Kutuzov
Ivan Lavrentiev
Robert McNabb
G. Hilmar Gudmundsson
Huilin Li
Liss M. Andreassen
Abstract. Knowledge of the ice thickness distribution of glaciers and ice caps is an important prerequisite for many glaciological and hydrological investigations. A wealth of approaches has recently been presented for inferring ice thickness from characteristics of the surface. With the Ice Thickness Models Intercomparison eXperiment (ITMIX) we performed the first coordinated assessment quantifying individual model performance. A set of 17 different models showed that individual ice thickness estimates can differ considerably – locally by a spread comparable to the observed thickness. Averaging the results of multiple models, however, significantly improved the results: on average over the 21 considered test cases, comparison against direct ice thickness measurements revealed deviations on the order of 10 ± 24 % of the mean ice thickness (1σ estimate). Models relying on multiple data sets – such as surface ice velocity fields, surface mass balance, or rates of ice thickness change – showed high sensitivity to input data quality. Together with the requirement of being able to handle large regions in an automated fashion, the capacity of better accounting for uncertainties in the input data will be a key for an improved next generation of ice thickness estimation approaches.
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